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HomeMy WebLinkAboutSW6170401 - The Crossings at Cumberland (6) a Stormwater Calculations For Project: The Crossings at Cumberland Fayetteville, NC Owner: Cumberland AL Investors, LLC , r r ►rrr O �. SEAL ` NGIPIE� <c, Prepared by: 61_!IJI ENGINEERING -SURVEYING - DESIGNING - DRAFTING Larry King & Associates, R.L.S., P.A. P.O. Box 53787 1333 Morganton Road, Suite 201 Fayetteville, North Carolina 28305 P. (910) 483-4300 F. (910) 483-4052 www.LKandA.com Firm License #: C-887 , f TABLE OF CONTENTS Stormwater Narrative SC-1 Infil. Basin #1 WQV Calculations SC-2 Time to Peak Calculations - Post-Development SC-3 Pond Volumes SC-4 Infil. Basin#2 WQV Calculations SC-5 Time to Peak Calculations - Post-Development SC-6 Pond Volumes SC-7 Infil. Basin #3 WQV Calculations SC-8 Time to Peak Calculations - Post-Development SC-9 Pond Volumes SC-10 Pond Volumes SC-11 - Basin Routing Calculations APPENDIX A Misc. Erosion Control Calculations APPENDIX B Site Maps APPENDIX C Soils Report APPENDIX D Site Deed APPENDIX E 1 STORMWATER NARRATIVE This project is a proposed assisted living facility located on an undeveloped 7 acre +/- parcel. The undeveloped parcel is at 7051 Rockfish Road. It is bounded by single-family residential to the east and north and undeveloped rural land to the south and west. The site is planned to utilize three infiltration basins places around the site to capture runoff from the parking lots and building. Six separate soil bores were taken around the site to determine seasonal high . water table depths and infiltration rates. Bores were initially taken in the middle of anticipated basin locations, but basin locations changed as the project evolved. Overall, the site has very good infiltration rates varying between 0.51 in/hr and 11.52 in/hr. Bores adjacent to Infiltration Basin #1 tested at 10.88 in/hr with another bore showing 0.51 in/hr. Basin #1 is designed with an assumed 0.5 in/hr. The bore for Basin#2 range is 3.14 in/hr. The basin is designed with an assumed 2 in/hr. Bores adjacent to Basin #3 range from 3.89 in/hr to 11.52 in/hr. The basin is designed with an assumed 3 in/hr. A stormwater access easement is provided for maintenance access to the wet detention basin. Supplemental calculations are attached. i SC-1 � 1 on ENGINEERING-SURVEYING-DESIGNING-DRAFTING Larry King & Associates, R.L.S., P.A. P. (910) 483-4300 www.LKandA.com F. (910) 483-4052 Water Quality Volume Calculation Project Name: P 16.420E he �ross`ings„at C rii r nd.`. Outlet: ,DA'',41.g,F;s:R11510,00 Calculate Runoff Coefficient A= 2.12 acreszR:: 92;'1`67 sf Watershed area Ai= 1 04 acres uRag-14, sf Impervious area la= 0.49 Impervious fraction Rv=0.05+0.9*la Rv= 0.49 Runoff Coefficient Calculate Runoff Volume Required to be Controlled Rd=3%31:::]=41!in Design storm rainfall depth (typically 1” or 1.5") V=3630*Rd*Rv*A WQV= 3,790 cf Volume of runoff that must be 1.04 Ac in controlled for specified design storm Calculate Required Pond Surface Area for Infiltration System SA=DV/(FS*(K*T)) SA=Surface Area (sf) DV=Design Volume s 612 1 4' :cf(10yr Volume) FS=Factor of Safety ' K= Hydraulic Conductivity of Soilnz 'T' :` 5 in/hr T=Max Dewatering TimeF%a ` °"r .72r hrs SA= 377.0 sf Required Surface Area Drawdown Times T=DV/(FS*(K*SA)) SA=Surface Area (sf) -°°,76£92°sf(Bottom of Pond) DV=Design Volume 4 ,; °3'79p'Fcf(1"WQV) DV=Design Volume 'r 27,:145jcf(10yr Volume) FS=Factor of Safety K= Hydraulic Conductivity of Soil '_; r �0151 in/hr T= 1.00 hr for 1"WQV T= 7.14 hr for 10yr Volume SC-2 , r ENGINEERING-SURVEYING-DESIGNING-DRAFTING Larry King & Associates, R.L.S., P.A. P. (910) 483-4300 www.LKandA.com F. (910) 483-4052 Time to Peak Calculations Project Name: P16-120 The Crossings at Cumberland Outlet: DA-1 Calculate Time to Peak&Volume of Runoff QP °x:. ;96)cfs DA= ; x2`1,2a acres Rational C=s{: '1 x xe0 6 P=.17,41201' >` 1701 in (10yr/24hr storm) . Cn=ab+cx"d a= 50.82581 b+xAd b= 1.461704 c= 165.6338 d= 1.350661 Cn= 80 x= Rational C S= 2.48 (1000/CN)-10 Q.= 3.53 in TP 33.76 min Volume of Runoff(10 Year Storm) Vol=1.39*Qp*Tp Vol= 27,145 cf Hydrograph Shape t ;;:;.,.; 6 min Ascending limb= 5.63 Decending limb= 9.40 SC-3 on ENGINEERING-SURVEYING-DESIGNING-DRAFTING Larry King & Associates, R.L.S., P.A. P. (910) 483-4300 www.LKandA.com F. (910) 483-4052 Pond Volume Calculations Project Name: P16-120 The Crossings at Cumberland Outlet: DA-1 Infiltration Basin Forebay Volume Required Elev. Contour Accum. Contour Accum. Stage Diff Area Incr.Vol. Vol. Stage Elev.Diff Area Incr.Vol. Vol. (ft) (ft) NO (cf) (cf) (ft) (ft) (sf) (cf) (cf) 178 0.0 7,602 0 0 178 0.0 7,602 0 0 179 1.0 10,151 8,877 8,877 179 1.0 10,151 8,877 8,877 180 1.0 12,865 11,508 20,385 180 1.0 12,865 11,508 20,385 181 1.0 15,718 14,292 34,676 20%of Volume 4,077 Forebay Volume Provided 4,270 20.9% Forebay Elev. Contour Accum. Stage Diff Area Incr.Vol. Vol. (ft) (ft) (St) (cf) (cf) 178 0.0 1,305 0 0 179 1.0 2,100 1,703 1,703 180 1.0 3,034 2,567 4,270 20%of Volume 4,077 SC-4 ® ENGINEERING-SURVEYING-DESIGNING-DRAFTING Larry King & Associates, R.L.S., P.A. P. (910) 483-4300 www.LKandA.com F. (910) 483-4052 Water Quality Volume Calculation Project Name: xP1:61201Ttie"Clossiri satFCu% fberlandx' Outlet: Calculate Runoff Coefficient A= 2.02 acres tr 216; sf Watershed area Ai= 1 09 acres . :4.7 35p.sf Impervious area la= - 0.54 Impervious fraction Rv=0.05+0.9*la Rv= 0.53 Runoff Coefficient Calculate Runoff Volume Required to be Controlled Rd i':4],71'!1•011.,„ ;I in Design storm rainfall depth (typically 1”or 1.5") V=3630*Rd*Rv*A WQV= 3,918 cf Volume of runoff that must be 1.08 Ac in controlled for specified design storm Calculate Required Pond Surface Area for Infiltration System SA=DV/(FS*(K*T)) SA=Surface Area (sf) DV=Design Volume ,'2`6'58i cf(10yr Volume) FS=Factor of Safety K= Hydraulic Conductivity of Soil ;" 3,in/hr T=Max Dewatering Time " x :'.r' °=72°hrs SA= 61.5 sf Required Surface Area Drawdown Times T=DV/(FS*(K*SA)) SA=Surface Area (sf) '=:7602;sf(Bottom of Pond) DV=Design Volume L3,y918',cf(1"WQV) DV=Design Volume ' 13 324.cf(10yr Volume) FS=Factor of Safety K= Hydraulic Conductivity of Soil '3 in/hr T= 0.17 hr for 1"WQV T= 0.58 hr for 10yr Volume SC-5 ENGINEERING-SURVEYING-DESIGNING-DRAFTING Larry King & Associates, R.L.S., P.A. P. (910) 483-4300 www.LKandA.com-F. (910) 483-4052 Time to Peak Calculations Project Name: P16-120 The Crossings at Cumberland Outlet: DA-2 Calculate Time to Peak&Volume of Runoff QP i x' %; Rx97 cfs DA= ; rxg2x.0Z acres Rational C= ?Fx 'xKx02 P= .'i ', r5`° Q4in (10yr/24hr storm) . :SRR Cn=ab+cx^d a= 50.82581 b+x^d b= 1.461704 c= 165.6338 d= 1.350661 Cn= 81 x= Rational C S= 2.33 (1000/CN)-10 Q'= 3.62 in TP 32.89 min Volume of Runoff(10 Year Storm) Vol=1.39 *Qp*Tp Vol= 26,581 cf Hydrograph Shape tc=«<.4:. ,<: 6§min Ascending limb= 5.48 Decending limb= 9.15 • SC-6 { on ENGINEERING-SURVEYING-DESIGNING-DRAFTING Larry King & Associates, R.L.S., P.A. P. (910) 483-4300 www.LKandA.com F. (910) 483-4052 Pond Volume Calculations Project Name: P16-120 The Crossings at Cumberland Outlet: DA-2 Infiltration Basin Forebay Volume Required Elev. Contour Accum. Contour Accum. Stage Diff Area Incr.Vol. Vol. Stage Elev.Diff Area Incr.Vol. Vol. (ft) (ft) (sf) (cf) (cf) (ft) (ft) (sf) (cf) (cf) 178 6 0 0 13,324 0 0 178.6 0.0 13,324 0 0 179.5 0.9 16,088 13,235 13,235 179.5 0 9 16,088 13,235 13,235 180 5 1 0 19,213 17,651 30,886 180 0.5 17,345 8,358 21,594 20%of Volume 4,319 Forebay Volume Provided 4,230 19 6% Forebay East Elev. Contour Accum. Stage Diff Area Incr.Vol. Vol. (ft) (ft) (sf) (cf) (cf) 178.6 0.0 962 0 0 179 0.4 1,132 419 419 180 1.0 1,734 1,433 1,852 43%of Volume 1,857 Forebay West Elev. Contour Accum. Stage Diff Area Incr.Vol. Vol. (ft) (ft) (sf) (cf) (CO 178.6 0.0 1,300 0 0 179 0.4 1,519 564 564 180 1.0 2,109 1,814 2,378 57%of Volume 2,289 SC-7 ® ENGINEERING-SURVEYING-DESIGNING-DRAFTING Larry King & Associates, R.L.S., P.A. P. (910) 483-4300 www.LKandA.com F. (910) 483-4052 Water Quality Volume Calculation Project Name: rP,16120TIe Crossings at%=runberland.'' Outlet: Calculate Runoff Coefficient A= 1.56 acres oi68,0481 sf Watershed area Ai= 0.70 acres , .x`'30;447 sf Impervious area la= 0.45 Impervious fraction Rv=0.05+0.9*Ia Rv= 0 45 Runoff Coefficient Calculate Runoff Volume Required to be Controlled Rd=i.:!:-1;,:igiE5Et in Design storm rainfall depth (typically 1"or 1.5") V=3630*Rd*Rv*A WQV= 2,567 cf Volume of runoff that must be 0.71 Ac in controlled for specified design storm Calculate Required Pond Surface Area for Infiltration System SA=DV/(FS*(K*T)) SA=Surface Area (sf) DV=Design Volume .;;1'5;829 cf(10yr Volume) FS=Factor of Safety = 2° K= Hydraulic Conductivity of Soil „„%°,s ,.Y2e in/hr T=Max Dewatering Time .' 72x'hrs SA= 55.0 sf Required Surface Area Drawdown Times T=DV/(FS*(K*SA)) SA=Surface Area (sf) ` ::';;:8;633 sf(Bottom of Pond) DV=Design Volume 12567,cf(1"WQV) DV=Design Volume ;x z 15,830;cf(10yr Volume) FS=Factor of Safety K= Hydraulic Conductivity of Soil "i'4.2(in/hr T= 0.15 hr for 1"WQV T= 0.92 hr for 10yr Volume SC-8 A on ENGINEERING-SURVEYING-DESIGNING-DRAFTING Larry King & Associates, R.L.S., P.A. P. (910) 483-4300 www.LKandA.com F. (910) 483-4052 Time to Peak Calculations Project Name: P16-120 The Crossings at Cumberland Outlet: DA-3 Calculate Time to Peak&Volume of Runoff Qp= 5 4 cfs DA= ,:;;Ai4;i14'i.56 acres Rational C=Alvj0-545:i P= 5 70 in (10yr/24hr storm) Cn=ab+cx^d a= 50.82581 b+x^d b= 1.461704 c= 165.6338 d= 1.350661 Cn= 72 x= Rational C S= 3.79 (1000/CN)-10 Q*= 2.80 in Tp= 35.41 min Volume of Runoff(10 Year Storm) Vol=1.39*Qp*Tp Vol= 15,829 cf Hydrograph Shape tc= 01 min Ascending limb= 5.90 Decending limb= 9.86 SC-9 on ENGINEERING-SURVEYING-DESIGNING-DRAFTING Larry King & Associates, R.L.S., P.A. P. (910) 483-4300 www.LKandA.com F. (910) 483-4052 Pond Volume Calculations Project Name: P16-120 The Crossings at Cumberland Outlet: DA-3 Infiltration Basin Forebay Volume Required Elev. Contour Accum. Contour Accum. Stage Diff Area Incr.Vol. Vol. Stage Elev.Diff Area Incr.Vol. Vol. (ft) (ft) (Sfl (cf) (cf) (ft) (ft) (sf) (cf) (cf) 178 0 0 8,633 0 0 178 0.0 8,633 0 0 179 1.0 13,095 10,864 10,864 179 1.0 13,095 10,864 10,864 1.80 1.0 17,735 15,415 26,2.79 179 5 0.5 15,401 7,124 17,988 20%of Volume 3,598 Forebay Volume Provided 3,692 20 5% Forebay West Elev. Contour Accum. Stage Diff Area Incr.Vol. Vol. (ft) (ft) (Sfl (cf) (cf) 178 0.0 997 0 0 179 1.0 1,721 1,359 1,359 179 5 0.5 2,143 966 2,325 60%of Volume 2,159 Forebay East Elev. Contour Accum. Stage Diff Area Incr.Vol. Vol. (ft) (ft) NO (cf) (CO 178 0.0 561 0 0 179 1.0 1,019 790 790 179.5 0.5 1,290 577 1,367 40%of Volume 1,439 SC-10 Drainage Areas Breakdown 1 otal Area- l�i<FI.o",mryn°rg,esm,,",p�n�,'%'A'A,',�•�<rt,e.a:;1i.'t?w"r�v� 6C�.r�7x,�7'";:"=: ;,s.ti�f,�3J;��:i�,t�,,;`:t.G�nszFa.,,FdtJi,-4,.i�;:jY t:;,^g`G3���'.F"i.N;,-,ti."p`t,;.y;.«'f.;"s2�„:,s-Gr,.3„';..T..sa3,,';.I,c,i„=;.S.Y ;..;LF cilalw92,187IsR ' ; '” ,r7e6*p4` 45,409 e .„- , 6,11 6t „m.,.Y,.,}/.y�► A^/ .-, _ .„„.„« �„,:,r���t.,Vic”' as§"�TI�;".Niitt,��7""� ���`�y:���w-«y.W'�,`..`W_ „b"«, a8, ','F�;:�m�<.. :�.. ,"�7{ >,vs 1.757, 2=tac noalAea- 88,125 fI pAfeaa,,, 47350isfk" , alu ,et,,ti,>` •Are1 , : '��"t;,,; „� zgt "rq.Gn£` �- s fi,,`:;mr•. ='me.;,,�,,�; .rr....,, M�'"�''r Total Are 68,04o s � 4,„4,41,0„,,,,,,•' ,d�•. x '� 'f. S`t;Yn;,'"3^" .`.ssk.%;+ ,dx4.=d o-,>:� I Are` 30 447 is r:`; `'�t3�;:". �,;i "'". ;°;;: �'St �°;1''' P,,e Com C . - ', 0.5 SC-11 b xipuaddy • Table of Contents The Crossings at Cumberland gpw Hydraflow Hydrographs by Intelisolve Friday,Mar 31 2017, 1 37 PM Hydrograph Return Period Recap 1 1 - Year Summary Report 2 Hydrograph Reports 3 Hydrograph No. 1, Rational, DA-2 3 Hydrograph No. 2, Rational, DA-3 4 Hydrograph No. 3, Reservoir, DA-2 POST 5 Pond Report 6 Hydrograph No. 4, Reservoir, DA-3 POST 7 Pond Report 8 Hydrograph No. 5, Rational, DA 1 9 Hydrograph No. 6, Reservoir, DA-1 POST 10 Pond Report 11 10 - Year Summary Report 12 Hydrograph Reports 13 Hydrograph No. 1, Rational, DA-2 13 Hydrograph No. 2, Rational, DA-3 14 Hydrograph No. 3, Reservoir, DA-2 POST 15 Pond Report 16 Hydrograph No. 4, Reservoir, DA-3 POST 17 Pond Report 18 Hydrograph No. 5, Rational, DA 1 19 Hydrograph No. 6, Reservoir, DA-1 POST 20 Pond Report 21 100 - Year Summary Report 22 Hydrograph Reports 23 Hydrograph No. 1, Rational, DA-2 23 Hydrograph No. 2, Rational, DA-3 24 Hydrograph No. 3, Reservoir, DA-2 POST 25 Pond Report 26 Hydrograph No. 4, Reservoir, DA-3 POST 27 Pond Report 28 Hydrograph No. 5, Rational, DA 1 29 Hydrograph No. 6, Reservoir, DA-1 POST 30 Pond Report 31 '1 Hydrograph Return Period Recap Hyd. Hydrograph Inflow Peak Outflow(cfs) Hydrograph No. type Hyd(s) description (origin) 1-Yr 2-Yr 3-Yr 5-Yr 10-Yr 25-Yr 50-Yr 100-Yr 1 Rational ----- 6 17 — -- — 9.49 12 36 DA-2 2 Rational 3 48 ------ 5 36 6 97 DA-3 3 Reservoir 1 0 62 ----- 0.70 0 78 DA-2 POST 4 Reservoir 2 0 66 ------ 0 94 1 02 DA-3 POST 5 Rational ----- 6 27 9 64 12 55 DA 1 6 Reservoir 5 0 14 0 16 0 18 DA-1 POST Pro]. file: The Crossings at Cumberland.gpw Friday, Mar 31 2017, 1 :37 PM Hydraflow Hydrographs by Intel'solve 4 2 Hydrograph Summary Report Hyd. Hydrograph Peak Time Time to Volume Inflow Maximum Maximum Hydrograph No. type flow interval peak hyd(s) elevation storage description (origin) (cfs) (min) (min) (cuft) (ft) (cuft) 1 Rational 6.17 1 33 16,246 ---- ----- DA-2 2 Rational 3.48 1 35 9,873 ---- DA-3 3 Reservoir 0.62 1 82 15,896 1 179 56 14,122 DA-2 POST 4 Reservoir 0 66 1 83 9,802 2 178 72 7,849 DA-3 POST 5 Rational 6.27 1 34 16,952 ---- DA 1 6 Reservoir 0 14 1 89 14,649 5 179 64 16,255 DA-1 POST The Crossings at Cumberland.gpw Return Period: 1 Year Friday, Mar 31 2017, 1 :37 PM Hydraflow Hydrographs by Intelisolve 3 Hydrograph Plot Hydraflow Hydrographs by Intehsolve Friday,Mar 31 2017, 1 37 PM Hyd. No. 1 DA-2 Hydrograph type = Rational Peak discharge = 6.17 cfs Storm frequency = 1 yrs Time interval = 1 min Drainage area = 2.020 ac Runoff coeff. = 0.62 Intensity = 4.926 in/hr Tc by User = 6.00 min IDF Curve, = City of Fayetteville IDF.IDF Asc/Rec limb fact = 5.48/9.15 Hydrograph Volume=16,246 cuft DA-2 Q (cfs) Hyd No. 1 -- 1 Yr Q (cfs) 7.007 00 6.00 6.00 5.00 5.00 4.00 4 00 3.00 3 00 2.00 2.00 1.00 1 00 0 00 0.00 0.0 0.2 0.3 0 5 0.7 0 8 1.0 1 2 1 3 1 5 Time (hrs) Hyd No 1 4 Hydrograph Plot Hydraflow Hydrographs by Intel'solve Friday,Mar 31 2017, 1.37 PM Hyd. No. 2 DA-3 Hydrograph type = Rational Peak discharge = 3.48 cfs Storm frequency = 1 yrs Time interval = 1 min Drainage area = 1.570 ac Runoff coeff. = 0.45 Intensity = 4.926 in/hr Tc by User = 6.00 min IDF Curve = City of Fayetteville IDF.IDF Asc/Rec limb fact = 5.9/9.86 Hydrograph Volume=9,873 cuft DA-3 Q (cfs) Hyd No. 2 -- 1 Yr Q (cfs) 4.00 4.00 3.00 3.00 2.00 2.00 1.00 1.00 0.00 0 00 00 02 03 05 07 08 10 12 13 15 17 Time (hrs) Hyd No. 2 5 Hydrograph Plot Hydraflow Hydrographs by Intel'solve Friday,Mar 31 2017, 1 37 PM Hyd. No. 3 DA-2 POST Hydrograph type = Reservoir Peak discharge = 0.62 cfs Storm frequency = 1 yrs Time interval = 1 min Inflow hyd. No. = 1 Max. Elevation = 179.56 ft Reservoir name = Infil Basin #2 Max. Storage = 14,122 cuft Storage Indication method used. Hydrograph Volume=15,896 cult DA-2 POST Q (cfs) Hyd. No 3-- 1 Yr Q (cfs) 700 700 6.00 ( 6.00 - 5.00 5 00 4 00 4 00 3.00 3 00 2.00 2.00 \ __ _ __ _ _ 1.00 1.00 0.00 0.00 0 3 6 9 12 15 18 21 24 27 30 Time (hrs) Hyd No. 3 Hyd No. 1 1 Pond Report 6 Hydraflow Hydrographs by Intelisolve Friday,Mar 31 2017,1 37 PM Pond No. 3 - Infil Basin#2 . , Pond Data Pond storage is based on known contour areas. Average end area method used. Stage/Storage Table Stage(ft) Elevation(ft) Contour area(sqft) Incr.Storage(cuft) Total storage(cuft) 0 00 178 60 13,100 0 0 0 90 179 50 15,831 13,019 13,019 1 90 180 50 18,927 17,379 30,398 Culvert/Orifice Structures Weir Structures [A] [B] [C] [D] [A] [B] [C] [D] Rise(in) = 0.00 0.00 0 00 0 00 Crest Len(ft) = 0 00 0 00 0 00 0 00 • Span(in) = 0.00 0 00 0.00 0 00 Crest El.(ft) = 0 00 0 00 0 00 0 00 No.Barrels = 0 0 0 0 Weir Coeff. = 0 00 0 00 0.00 0 00 Invert El.(ft) = 0 00 0 00 0 00 0 00 Weir Type = --- --- --- --- Length(ft) = 0 00 0 00 0 00 0 00 Multi-Stage = No No No No Slope(%) = 0 00 0 00 0.00 0 00 N-Value = 000 .000 000 .000 Orif.Coeff. ' = 0 00 0 00 0.00 0 00 Multi-Stage = n/a No No No Exfiltration= 2 000 in/hr(Contour) Tailwater Elev = 0 00 ft Note Culvert/Orifice outflows have been analyzed under inlet and outlet control Stage(ft) Stage/Discharge Stage(ft) 2 00 2 00 1 80 1 80 1 60 1 60 1.40 1 40 1.20 1 20 1.00 1 00 0 80 0 80 0 60 '� 0 60 0.40 0.40 020 020 0.00 0 00 0 00 0 10 0 20 0 30 0 40 0 50 0 60 0 70 0 80 0 90 1 00 Discharge(cfs) Total Q , 7 Hydrograph Plot Hydraflow Hydrographs by Intel'solve Friday, Mar 31 2017, 1 37 PM Hyd. No. 4 DA-3 POST Hydrograph type = Reservoir Peak discharge = 0.66 cfs Storm frequency = 1 yrs Time interval = 1 min Inflow hyd. No. = 2 Max. Elevation = 178.72 ft Reservoir name = Infil Basin #3 Max. Storage = 7,849 cult Storage Indication method used. Hydrograph Volume=9,802 cuft DA-3 POST Q (cfs) Hyd. No. 4-- 1 Yr Q (cfs) 4.00 4 00 1 - 3.00 3.00 2.00 2.00 1.00 1.00 0.00 ___ 0.00 0.0 1.7 3.3 5.0 6.7 8.3 10.0 11.7 13.3 15.0 167 183 • Time (hrs) Hyd No. 4 Hyd No. 2 A Pond Report 8 Hydraflow Hydrographs by Intelisolve Friday, Mar 31 2017, 1 37 PM Pond No. 4 - Infil Basin#3 Pond Data Pond storage is based on known contour areas Average end area method used Stage/Storage Table Stage(ft) Elevation(ft) Contour area(sqft) Incr.Storage(cuft) Total storage(cuft) 0.00 178 00 8,633 0 0 1 00 179 00 13,095 10,864 10,864 2 00 180.00 17,735 15,415 26,279 Culvert/Orifice Structures Weir Structures [A] [B] [C] [D] [A] [B] - [C] [D] Rise(in) = 0 00 0 00 0 00 0 00 Crest Len(ft) = 0 00 0.00 0.00 0 00 Span(in) = 0.00- 0 00 0 00 0 00 Crest El.(ft) = 0 00 0 00 0 00 0 00 No.Barrels = 0 0 0 0 Weir Coeff. = 0 00 0 00 0 00 0 00 Invert El.(ft) = 0 00 0 00 0 00 0 00 Weir Type = --- --- --- Length(ft) = 0 00 0 00 0 00 0.00 Multi-Stage = No No No No Slope(%) = 0 00 0 00 0 00 0 00 N-Value = .000 000 .000 000 Orif.Coeff. = 0 00 0.00 0 00 0 00 Multi-Stage = n/a No No No Exfiltration= 3 000 in/hr(Contour) Tailwater Elev = 0 00 ft Note Culvert/Orifice outflows have been analyzed under inlet and outlet control Stage(ft) Stage/ Discharge Stage(ft) 200 200 1.80 1 80 1.60 1 60 1.40 1 40 1 20 1 20 1.00 1.00 0.80 0 80 060 060 0.40 0 40 0.20 0 20 000 000 0.00 0 50 1 00 1 50 2 00 Discharge(cfs) Total Q • , 9 Hydrograph Plot Hydraflow Hydrographs by Intelisolve Friday,Mar 31 2017, 1 37 PM 1 Hyd. No. 5 DA 1 Hydrograph type = Rational Peak discharge = 6.27 cfs Storm frequency = 1 yrs Time interval = 1 min Drainage area . = 2.120 ac Runoff coeff. = 0.6 Intensity = 4.926 in/hr Tc by User = 6.00 min IDF Curve = City of Fayetteville IDF.IDF Asc/Rec limb fact = 5.63/9.4 Hydrograph Volume= 16,952 cuft DA 1 Q (cfs) Hyd. No 5 -- 1 Yr Q (cfs) 7.00 7.00 6 00 6 00 5.00 5 00 4 004.00 3.00 3:00 2.00 2 00 1.00 1.00 0.00 0 00 0.0 0.2 0.3 0 5 0 7 0 8 1.0 1.2 1.3 1.5 Time (hrs) Hyd No. 5 10 Hydrograph Plot Hydraflow Hydrographs by Intel'solve Friday,Mar 31 2017, 1'37 PM Hyd. No. 6 DA-1 POST Hydrograph type = Reservoir Peak discharge = 0.14 cfs Storm frequency = 1 yrs Time interval = 1 min Inflow hyd. No. = 5 Max. Elevation = 179.64 ft Reservoir name = Infil Basin #1 Max. Storage = 16,255 cult Storage Indication method used Hydrograph Volume=14,649 cuft DA-1 POST Q (cfs) Hyd. No. 6 -- 1 Yr Q (cfs) 7.00 7.00 6.00 I6.00 5.00 5.00 4 00 4.00 3.00 3 00 2.00 2.00 1.00 1 00 0.00 -- • 0.00 0 5 10 15 19 24 29 34 39 44 48 Time (hrs) Hyd No 6 Hyd No. 5 Pond Report 7i Hydraflow Hydrographs by Intelisolve Friday, Mar 31 2017, 1 37 PM Pond No. 2 - Infil Basin#1 Pond Data Pond storage is based on known contour areas Average end area method used Stage/Storage Table Stage(ft) Elevation(ft) Contour area(sqft) Incr.Storage(cuft) Total storage(cuft) 0 00 178 00 7,596 0 0 1 00 179 00 10,157 8,877 8,877 2 00 180 00 12,875 11,516 20,393 3.00 181 00 15,750 14,313 34,705 Culvert/Orifice Structures Weir Structures [A] [B] [C] [D] [A] [B] [C] [D] Rise(in) = 0 00 0.00 0 00 0.00 Crest Len(ft) = 0 00 0 00 0 00 0 00 Span(in) = 0.00 0 00 0.00 0 00 Crest El.(ft) = 0.00 0 00 0 00 0 00 No.Barrels = 0 0 0 0 Weir Coeff. = 0 00 0 00 0.00 0 00 Invert El.(ft) = 0 00 0 00 0 00 0 00 Weir Type = --- --- --- --- Length(ft) = 0.00 0 00 0.00 0 00' Multi-Stage = No No No No Slope(%) = 0 00 0 00 0 00 0 00 ' N-Value = 000 000 000 000 Orif.Coeff. = 0 00 0.00 0 00 0.00 Multi-Stage = n/a No No No Exfiltration= 0 500 in/hr(Contour) Tapwater Elev = 0 00 ft Note Culvert/Onfice outflows have been analyzed under inlet and outlet control Stage(ft) Stage/Discharge Stage(ft) 3.00 3 00 200 200 1.00 1 00 0.00 0 00 0 00 0 10 0 20 0 30 0 40 0 50 0 60 0 70 0 80 0 90 1 00 Discharge(cfs) Total Q 12 Hydrograph Summary Report Hyd. Hydrograph Peak Time Time to Volume Inflow Maximum Maximum Hydrograph No. type flow interval peak hyd(s) elevation storage description , (origin) (cfs) (min) (min) (cuft) (ft) (cuft) 1 Rational 9 49 1 33 24,999 ---- ----- , DA-2 2 Rational 5.36 1 35 15,192 ---- DA-3 3 Reservoir 0.70 1 83 24,471 1 180 03 22,203 DA-2 POST 4 Reservoir 0.94 1 84 15,090 2 179 08 12,141 DA-3 POST 5 Rational 9 64 1 34 26,085 ---- ----- ---- DA 1 6 Reservoir 0 16 1 89 21,149 5 180 33 25,170 DA-1 POST The Crossings at Cumberland.gpw Return Period: 10 Year Friday, Mar 31 2017, 1 :37 PM Flvdraflow Hvdroaraphs by Intelisolve t 13 Hydrograph Plot Hydraflow Hydrographs by Intelisolve Friday,Mar 31 2017, 1 37 PM Hyd. No. 1 DA-2 Hydrograph type = Rational Peak discharge = 9.49 cfs Storm frequency = 10 yrs Time interval = 1 min Drainage area = 2.020 ac Runoff coeff. = 0.62 Intensity = 7.580 in/hr Tc by User = 6.00 min IDF Curve = City of Fayetteville IDF.IDF Asc/Rec limb fact = 5.48/9.15 Hydrograph Volume=24,999 cuft DA-2 Q (cfs) Hyd No. 1 -- 10 Yr Q (cfs) 10.00 10.00 8.00 8 00 6.00 6.00 4.00 4.00 2.00 - 2.00 0.00 0.00 0.0 0.2 0 3 0 5 0.7 0 8 1 0 1 2 1.3 1 5 Time (hrs) Hyd No. 1 t 14 Hydrograph Plot Hydraflow Hydrographs by Intel'solve Friday, Mar 31 2017, 1 37 PM Hyd. No. 2 DA-3 i Hydrograph type = Rational Peak discharge = 5.36 cfs Storm frequency = 10 yrs Time interval = 1 min 1 Drainage area = 1.570 ac Runoff coeff. = 0.45 Intensity = 7.580 in/hr Tc by User = 6.00 min IDF Curve = City of Fayetteville IDF.IDF Asc/Rec limb fact = 5.9/9.86 Hydrograph Volume=15,192 cult DA-3 Q (cfs) Hyd. No 2-- 10 Yr Q (cfs) 6.00 1 6 00 5 00 5.00 4.00 4 00 3.00 3 00 2.00 2.00 1.00 1 00 000 0.00 0 0 0.2 0.3 0.5 0 7 0 8 1.0 1.2 1.3 1 5 1.7 Time (hrs) Hyd No 2 • 15 Hydrograph Plot Hydraflow Hydrographs by Intelisolve Friday, Mar 31 2017, 1 37 PM Hyd. No. 3 DA-2 POST Hydrograph type = Reservoir Peak discharge = 0.70 cfs Storm frequency = 10 yrs Time interval = 1 min Inflow hyd. No. = 1 Max. Elevation = 180.03 ft Reservoir name = Infil Basin #2 Max. Storage = 22,203 cuft Storage Indication method used. Hydrograph Volume=24,471 cult DA-2 POST Q (cfs) Hyd. No 3-- 10 Yr Q (cfs) 10.00 10 00 8.00 8 00 6.00 6 00 4.00 4 00 2.00 - 2.00 r ----------____ 0.00 _ ..a... 0 00 0 3 6 10 13 16 19 22 25 29 32 35 Time (hrs) Hyd No. 3 Hyd No. 1 I 1 t Pond Report 16 Hydraflow Hydrographs by Intelisolve Friday, Mar 31 2017, 1 37 PM Pond No. 3 - Infil Basin#2 Pond Data Pond storage is based on known contour areas Average end area method used Stage/Storage Table Stage(ft) Elevation(ft) Contour area(sqft) Incr.Storage(cuft) Total storage(cuft) 0 00 178 60 13,100 0 0 0.90 179 50 15,831 13,019 13,019 1 90 180 50 18,927 17,379 30,398 Culvert/Orifice Structures Weir Structures [A] [B] [C] [D] [A] [B] [C] [D] Rise(in) = 0 00 0.00 0 00 0 00 Crest Len(ft) = 0 00 0 00 0 00 0 00 Span(in) = 0 00 0 00 0 00 0 00 Crest El.(ft) = 0 00 0 00 0 00 0 00 No.Barrels = 0 0 0 0 Weir Coeff. = 0.00 0.00 0 00 0.00 Invert El.(ft) = 0 00 0 00 0 00 0.00 Weir Type = --- --- --- --- Length(ft) = 0 00 0.00 0 00 0 00 Multi-Stage = No No No No Slope(%) = 0 00 0 00 0 00 0 00 N-Value = .000 000 000 000 Orif.Coeff. = 0 00 0.00 0 00 0.00 Multi-Stage = n/a No No No Exfiltration= 2 000 in/hr(Contour) Tailwater Elev = 0 00 ft Note Culvert/Orifice outflows have been analyzed under inlet and outlet control Stage(ft) Stage/ Discharge Stage(ft) 2 00 2 00 1 80 1 80 160 160 140 140 1 20 1 20 1 00 1.00 080 080 060 060 0.40 0 40 020 020 0.00 0 00 0 00 0.10 0 20 0 30 0 40 0 50 0 60 0 70 0 80 0 90 1 00 Discharge(cfs) Total Q 17 Hydrograph Plot Hydraflow Hydrographs by Intelisolve Friday, Mar 31 2017, 1 37 PM Hyd. No. 4 DA-3 POST Hydrograph type = Reservoir Peak discharge = 0.94 cfs Storm frequency = 10 yrs Time interval = 1 min Inflow hyd. No. = 2 Max. Elevation = 179.08 ft Reservoir name = Infil Basin #3 Max. Storage = 12,141 cuft Storage Indication method used Hydrograph Volume=15,090 cuft DA-3 POST Q (cfs) Hyd. No. 4-- 10 Yr Q (cfs) 6.00 6.00 -- ----- ---- - - -- - -- --- - ----- --- - -- -- - ---- -------- - ---- -- 500 500 4.00 4.00 3.00 3 00 2.00 2.00 1.00 1.00 0 00 0.00 00 1.7 3.3 50 6.7 83 10.0 117 13.3 150 16.7 183 Time (hrs) Hyd No. 4 Hyd No.-2 Pond Report 18 Hydraflow Hydrographs by Intelisolve Friday, Mar 31 2017,1 37 PM Pond No. 4 - Infil Basin#3 Pond Data Pond storage is based on known contour areas Average end area method used. Stage/Storage Table Stage(ft) Elevation(ft) Contour area(sqft) Incr.Storage(cuft) Total etorage(cuft) 0 00 178.00 8,633 0 0 1.00 179.00 13,095 10,864 10,864 2 00 180.00 17,735 15,415 26,279 Culvert/Orifice Structures Weir Structures [A] [B] [C] [D] [A] [B] [C] [D] Rise(in) = 0.00 0 00 0 00 0 00 Crest Len(ft) = 0 00 0 00 0 00 0 00 Span(in) = 0 00 0 00 0.00 0 00 Crest El.(ft) = 0 00 0 00 0 00 0 00 No.Barrels = 0 0 0 0 Weir Coeff. = 0.00 0 00 0 00 0 00 Invert El.(ft) = 0 00 0 00 0 00 0 00 Weir Type = --- --- --- --- Length(ft) = 0 00 0 00 0 00 0 00 Multi-Stage = No No No No Slope(%) = 0.00 0 00 0 00 0 00 N-Value = 000 000 000 000 Orif.Coeff. = 0 00 0.00 0 00 0 00 Multi-Stage = n/a No No No Exfiltration= 3 000 in/hr(Contour) Tai!water Elev.= 0 00 ft • Note Culvert/Orlfice outflows have been analyzed under inlet and outlet control • Stage(ft) Stage/Discharge Stage(ft) 2.00 2 00 1 80 1.80 160 160 140 140 1 20 1 20 100 100 0 80 0.80 060 060 040 040 0 20 0 20 0 00 0 00 0.00 0 50 1 00 1 50 2.00 Discharge(cfs) Total Q 19 Hydrograph Plot Hydraflow Hydrographs by Intelisolve Friday,Mar 31 2017, 1 37 PM Hyd. No. 5 DA 1 Hydrograph type ' = Rational Peak discharge = 9.64 cfs Storm frequency = 10 yrs Time interval = 1 min Drainage area = 2.120 ac Runoff coeff. = 0.6 Intensity = 7.580 in/hr Tc by User = 6.00 min IDF Curve = City of Fayetteville IDF.IDF Asc/Rec limb fact = 5.63/9.4 Hydrograph Volume=26,085 cuft DA 1 Q (cfs) Hyd. No. 5 -- 10 Yr Q (cfs) 10.00 10.00 8.00 8 00 600 600 4.00 4 00 2 00 2.00 0 00 0 00 00 02 03 0.5 07 08 10 12 13 1.5 Time (hrs) Hyd No. 5 20 Hydrograph Plot Hydraflow Hydrographs by Intelisolve Friday,Mar 31 2017, 1 37 PM Hyd. No. 6 DA-1 POST Hydrograph type = Reservoir Peak discharge = 0.16 cfs Storm frequency = 10 yrs Time interval = 1 min Inflow hyd. No. = 5 Max. Elevation = 180.33 ft Reservoir name = Infil Basin #1 Max. Storage = 25,170 cuft Storage Indication method used Hydrograph Volume=21,149 cuft DA-1 POST Q (cfs) Hyd. No. 6-- 10 Yr Q (cfs) 10.00 10.00 8.00 8.00 6.00 6 00 4 00 4.00 2 00 2.00 0.00 ' 1 - 0.00 0 5 10 15 19 24 29 34 39 .44 48 • Time (hrs) Hyd No 6 Hyd No 5 Pond Report 21 Hydraflow Hydrographs by Intelisolve Friday,Mar 31 2017, 1 37 PM Pond No. 2 - Infil Basin#1 Pond Data Pond storage is based on known contour areas Average end area method used. Stage/Storage Table Stage(ft) Elevation(ft) Contour area(sqft) Incr.Storage(cuft) Total storage(cuft) 0 00 178.00 7,596 0 0 1.00 179 00 10,157 8,877 8,877 2 00 180 00 12,875 11,516 20,393 3.00 181 00 15,750 14,313 34,705 Culvert/Orifice Structures Weir Structures [A] [B] [C] [D] [A] [B] [C] [D] Rise(in) = 0 00 0 00 0 00 0 00 Crest Len(ft) = 0 00 0 00 0 00 0 00 Span(in) = 0 00 0 00 0.00 0 00 Crest El.(ft) = 0 00 0 00 0 00 0 00 No. Barrels = 0 0 0 0 Weir Coeff. = 0 00 0 00 0 00 0 00 Invert El.(ft) = 0 00 0 00 0 00 0 00 Weir Type = --- --- --- Length(ft) = 0 00 0 00 0.00 0 00 Multi-Stage = No No No No Slope(%) = 0 00 0 00 0.00 0 00 N-Value = 000 000 000 000 Orif.Coeff. = 0 00 0.00 0 00 0 00 Multi-Stage = n/a No No No Exfiltration= 0 500 in/hr(Contour) Tapwater Elev = 0 00 ft Note CulverUOnfice outflows have been analyzed under inlet and outlet control Stage(ft) Stage/Discharge Stage(ft) 3.00 3.00 2 00 2 00 1 00 1 00 0.00 0 00 0 00 0 10 0 20 0 30 0 40 0 50 0.60 0 70 0 80 0 90 1 00 Discharge(cfs) Total Q 22 Hydrograph Summary Report Hyd. Hydrograph Peak Time Time to Volume Inflow Maximum Maximum Hydrograph No. type flow interval peak hyd(s) elevation storage description (origin) (cfs) (min) (min) (cult) (ft) (cult) 1 Rational 12 36 1 33 32,550 ---- ----- DA-2 2 Rational 6.97 1 35 19,781 ---- DA-3 3 Reservoir 0 78 1 84 31,869 1 180 44 29,289 DA-2 POST 4 Reservoir 1.02 1 85 19,651 2 179 34 16,181 DA-3 POST 5 Rational 12.55 1 34 33,964 ---- ---- DA 1 6 ' Reservoir 0 18 1 89 25,113 5 180 87 32,876 DA-1 POST The Crossings at Cumberland.gpw Return Period: 100 Year Friday, Mar 31 2017, 1:37 PM Hydraflow Hydroqraphs by Intelisolve 23 Hydrograph Plot Hydraflow Hydrographs by Intelisolve Friday,Mar 31 2017, 1 37 PM Hyd. No. 1 DA-2 Hydrograph type = Rational Peak discharge = 12.36 cfs " Storm frequency = 100 yrs Time interval = 1 min Drainage area = 2.020 ac Runoff coeff. = 0.62 Intensity = 9.870 in/hr Tc by User = 6.00 min IDF Curve = City of Fayetteville IDF.IDF Asc/Rec limb fact = 5.48/9.15 Hydrograph Volume=32,550 cuft DA-2 Q (cfs) Hyd. No 1 -- 100 Yr Q (cfs) 14 00 14 00 12.00 12 00 10.00 10.00 8.00 8.00 6.00 6.00 4.00 4.00 2.00 - 2.00 0.00 0 00 0.0 0.2 0 3 0.5 0.7 0 8 1 0 1 2 1 3 1 5 Time (hrs) Hyd No. 1 24 Hydrograph Plot Hydraflow Hydrographs by Intelisolve Friday,Mar 31 2017, 1'37 PM Hyd. No. 2 DA-3 Hydrograph type = Rational Peak discharge = 6.97 cfs Storm frequency = 100 yrs Time interval = 1 min Drainage area = 1.570 ac Runoff coeff. = 0.45 Intensity = 9.870 in/hr Tc by User = 6.00 min IDF Curve = City of Fayetteville IDF.IDF Asc/Rec limb fact = 5.9/9.86 Hydrograph Volume=19,781 cuft DA-3 Q (cfs) Hyd No 2 -- 100 Yr Q (cfs) 7.00 7 00 I 6.00 1 6.00 5 00 5.00 4.00 4.00 ---- - 1 - - i 3.00 3.00 2.00 200 ---- - - - - 1.00 1 00 000 0.00 0 0 0 2 0 3 0.5 0 7 0.8 1.0 1.2 1.3 1.5 1 7 Time (hrs) Hyd No. 2 25 Hydrograph Plot Hydraflow Hydrographs by Intelisolve Friday,Mar 31 2017, 1:37 PM Hyd. No. 3 DA-2 POST Hydrograph type = Reservoir Peak discharge = 0.78 cfs Storm frequency = 100 yrs Time interval = 1 min Inflow hyd. No. = 1 Max. Elevation = 180.44 ft Reservoir name = Infil Basin #2 Max. Storage = 29,289 cuft Storage Indication method used Hydrograph Volume=31,869 cuft DA-2 POST Q (cfs) Hyd. No 3-- 100 Yr Q (cfs) 14.00 14.00 12.00 I 12.00 10.00 -- 10.00 8 00 8 00 600 6.00 4.00 4 00 2 00 1 2.00 0.00 11 ---—_ 0.00 0 3 7 10 13 17 20 23 27 30 33 37 Time (hrs) Hyd No. 3 Hyd No. 1 Pond Report 26 Hydraflow Hydrographs by Intelisolve Friday,Mar 31 2017, 1 37 PM Pond No. 3 - Infil Basin#2 Pond Data ' Pond storage is based on known contour areas. Average end area method used Stage/Storage Table Stage(ft) Elevation(ft) Contour area(sqft) Incr.Storage(cult) Total storage(cult) 0.00 178.60 13,100 0 0 0 90 179 50 15,831 13,019 13,019 1 90 180 50 18,927 17,379 30,398 Culvert/Orifice Structures Weir Structures [A] [B] [C] [D] [A] [B] [C] [0] Rise(in) = 0 00 0 00 0 00 0.00 Crest Len(ft) = 0.00 0.00 0 00 0 00 Span(in) = 0.00 0 00 0 00 0 00 Crest El.(ft) = 0 00 0 00 0 00 0 00 No.Barrels = 0 0 0 0 Weir Coeff. = 0 00 0 00 0 00 0 00 Invert El.(ft) = 0 00 0 00 0 00 0 00 Weir Type = --- --- --- --- Length(ft) _.0 00 0 00 0 00 0 00 Multi-Stage = No No No No Slope(%) = 0 00 0 00 0 00 0 00 N-Value = 000 000 000 .000 Orif.Coeff. = 0 00 0 00 0 00 0 00 Multi-Stage = n/a No No No Exfiltration= 2 000 In/hr(Contour) Tapwater Elev.= 0 00 ft Note Culvert/Orifice outflows have been analyzed under inlet and outlet control Stage(ft) Stage/Discharge Stage(ft) 2.00 2 00 1 80 1.80 1 60 1.60 1 1 40 1 40 1 20 1 20 100 100 080 080 0.60 0 60 0 40 0 40 020 020 0.00 0 00 0 00 0 10 0 20 0 30 0 40 0 50 0 60 0 70 0 80 0 90 1 00 Discharge(cfs) Total Q 27 Hydrograph Piot Hydraflow Hydrographs by Intehsolve Friday,Mar 31 2017, 1:37 PM Hyd. No. 4 DA-3 POST Hydrograph type = Reservoir Peak discharge = 1.02 cfs Storm frequency = 100 yrs Time interval = 1 min Inflow hyd. No. = 2 Max. Elevation = 179.34 ft Reservoir name = Infil Basin #3 Max. Storage = 16,181 cuft Storage Indication method used Hydrograph Volume=19,651 cuft DA-3 POST Q (cfs) Hyd. No. 4-- 100 Yr Q (cfs) 7.00 7.00 6.00 6 00 5.00 5.00 4.004.00 3.00 3.00 2.00 2.00 1 00 — 1.00 0.00 - 0 00 0.0 18 37 5.5 73 9.2 11.0 128 147 165 18.3 Time (hrs) Hyd No. 4 Hyd No. 2 Pond Report 28 Hydraflow Hydrographs by Inteltsolve Friday,Mar 31 2017, 1.37 PM Pond No. 4 - Infil Basin#3 Pond Data Pond storage is based on known contour areas. Average end area method used Stage/Storage Table Stage(ft) Elevation(ft) Contour area(sqft) Incr.Storage(cuft) Total storage(cuft) 0 00 178.00 8,633 0 0 1 00 179 00 13,095 10,864 10,864 2.00 180 00 17,735 15,415 26,279 Culvert I Orifice Structures Weir Structures [A] • [B] [C] [D] [A] [B] [C] [D] Rise(in) = 0 00 0 00 0 00 0 00 Crest Len(ft) = 0 00 0 00 0 00 0 00 Span(in) = 0.00 0.00 0 00 0 00 Crest El.(ft) = 0 00 0 00 0.00 0.00 No.Barrels = 0 0 0 0 Weir Coeff. = 0.00 0 00 0 00 0 00 Invert El.(ft) = 0.00 0.00 0 00 0 00 Weir Type = --- — -- Length(ft) = 0.00 0 00 0.00 0 00 Multi-Stage = No No No No Slope(%) = 0.00 0 00 0 00 0 00 N-Value = 000 000 000 000 Orif.Coeff. = 0 00 0 00 0 00 0.00 Multi-Stage = n/a No No No Exfiltration= 3 000 in/hr(Contour) Tailwater Elev = 0.00 ft Note Culvert/Onfice outflows have been analyzed under inlet and outlet control Stage(ft) Stage/Discharge Stage(ft) 2 00 2 00 180 180 1 60 1 60 1.40 1 40 1.20 1 20 t 1.00 1 00 0 80 0 80 0.600.60 0.40 0.40 0 20 0 20 0.00 0 00 0 00 0 50 1 00 1 50 2 00 Discharge(cfs) Total Q 29 Hydrograph Plot Hydraflow Hydrographs by Intelisolve Friday,Mar 31 2017, 1 37 PM Hyd. No. 5 DA 1 Hydrograph type = Rational Peak discharge = 12.55 cfs Storm frequency = 100 yrs Time interval = 1 min Drainage area = 2.120 ac Runoff coeff. = 0.6 Intensity = 9.870 in/hr Tc by User = 6.00 min IDF Curve = City of Fayetteville IDF.IDF Asc/Rec limb fact = 5.63/9.4 Hydrograph Volume=33,964 cuft DA 1 Q (cfs) Hyd. No. 5 -- 100 Yr Q (cfs) 14.00 14 00 12.00 12 00 • 1000 1000 8.00 8 00 6 00 6.00 4.00 4.00 2 00 2 00 0.00 0 00 0.0 0.2 0.3 0.5 0.7 0 8 1.0 1 2 1.3 1 5 Time (hrs) Hyd No 5 30 Hydrograph Plot Hydraflow Hydrographs by Intel'solve Friday, Mar 31 2017, 1 37 PM Hyd. No. 6 DA-1 POST Hydrograph type = Reservoir Peak discharge = 0.18 cfs Storm frequency = 100 yrs Time interval = 1 min Inflow hyd. No. = 5 Max. Elevation = 180.87 ft Reservoir name = Infil Basin #1 Max. Storage = 32,876 cuft Storage Indication method used Hydrograph Volume=25,113 cuft DA-1 POST Q (cfs) Hyd. No 6 -- 100 Yr Q (cfs) 14.00 14.00 12.00 I 12.00 10 00 10 00 8 00 8 00 6 00 6.00 4.00 4 00 2 00 2.00 0.00 '"l 0.00 0 5 10 15 19 24 29. 34 39 44 48 Time (hrs) Hyd No. 6 Hyd No 5 Pond Report 31 Hydraflow Hydrographs by Intelisolve Friday, Mar 31 2017, 1 37 PM Pond No. 2 - Infil Basin#1 Pond Data . Pond storage is based on known contour areas Average end area method used Stage/Storage Table Stage(ft) Elevation(ft) Contour area(sqft) Incr.Storage(cuft) Total storage(cuft) 0.00 178 00 7,596 0 0 1.00 179 00 10,157 8,877 8,877 2 00 180.00 12,875 11,516 20,393 3 00 181 00 15,750 14,313 34,705 Culvert/Orifice Structures Weir Structures [A] [B] [C] [D] [A] [B] [C] [D] Rise(in) = 0 00 0 00 0 00 0 00 Crest Len(ft) = 0 00 0 00 0 00 0 00 Span(in) = 0 00 0 00 0 00 0 00 Crest El.(ft) = 0.00 0 00 0 00 0 00 No.Barrels = 0 0 0 0 Weir Coeff. = 0 00 0 00 0.00 0.00 Invert El.(ft) = 0 00 0 00 0 00 0.00 Weir Type = Length(ft) = 0 00 0 00 0 00 0 00 Multi-Stage = No No No No Slope(%) = 0 00 0 00 0 00 0.00 N-Value = .000 000 000 000 Orif.Coeff. = 0.00 0 00 0.00 0.00 Multi-Stage = n/a No No No Exfiltration= 0 500 in/hr(Contour) Tallwater Elev.= 0.00 ft Note CulverUOnfice outflows have been analyzed under inlet and outlet control Stage(ft) Stage/Discharge Stage(ft) 3.00 3 00 2 00 2 00 100 100 0.00 0 00 0 00 0 10 0 20 0.30 0.40 0 50 0 60 0 70 0 80 0 90 1 00 Discharge(cfs) Total Q , Appendix B F ti DESIGN OF RIPRAP OUTLET 'PROTECTION. User Input Data Calculated Value Designed By: .JAN, PE Date: 3/2812017 Checked By: Date: : _ Company: Larry King &Assoc Project Name: The Crossings at Cumberland Project No.: Site Location (City/Town) Fayetteville, NC Culvert Id. FES-1;FES-2 Total Drainage Area (acres) - Step 1. Determine the tailwater depth£i-or .channel,characteristics below the pipe outlet for the design capacity of the pipe. If the tailwater depth is less than half the outlet pipe diameter, it is classified minimum tailwater condition_ If it is greater than half the pipe diameter, it is classified maximum condition. Pipes that outlet onto wide flat areas with no defined channel are assumed to have a minimum tailwater condition unless reliable flood stage elevations show otherwise. Outlet pipe diameter, Do (in.) 18 Tailwater depth (in.) 0 Minimum/Maximum tailwater? Min TW (Fig. 8.06a) Discharge (cfs) 5.8 Velocity (ft./,$) - 3.2' Step 2. Based on the taihvater conditions determined in step 1, enter Figure 8.06a or Figure 8.06b,and determine d50 riprap size and minimum apron length ( .a). The dam,size is the median stone size in a well-graded riprap apron. Step S. Determine apron width at the pipe outlet, the apron shape, and the apron width at the outlet end from the same figure used in Step 2. Minimum TW Maximum TW KFigure,8:06a, Figure`8:06b; Riprap d50, (ft.) 0.3' 1 � Minimum apron length, La (it) 9 Apron width at pipe outlet (ft.) 4.5 4.5 Apron shape , Apron width at outlet end (ft.) 10.5 1.5 Step 4. Determine the maximum stone diameter: Clnux= '1.5 x '150 Minimum TW Maximum TW Max Stone Diameter, dmax (ft.) 0.45 0 Step 5. Determine the apron thickness: Apron thickness = 1.5 xrs,a Minimum TW Maximum TW Apron Thickness(ft.) _ 0.675 0 Step 6. Fit the riprap apron to the site by making it level for the minimum length, L . from Figure 8.06a or Figure 8.06b_ Extend the apron farther downstream and along channel banks until stability is assured. Keep the apron as straight as possible and align it with the flow of the receiving stream. Make any necessary alignment bends near the pipe outlet so that the entrance into the receiving stream is straight Some locations may require lining of the entire channel cross section to assure stability It may be necessary to increase the size of riprap where protection of the channel side slopes is necessary (Appendix 8.05)_ Where overfalls exist at pipe outlets or flows are excessive, a plunge pool should be considered, see page 8.06.8_ DESIGN OF RIPRAP OUTLET PROTECTION Userinput Data - Calculated Value , _ Designed By: JAN,.FE Date: -= 3/28/201.7 Checked By: . Date: - Company: ,Larry King &Assoc. _- Project Name: ;The Crossings at Cumberland Project No.,: _ - Site Location (City/Town) _ Fayetteville, NC Culvert Id. Infil Basin #2 - Total Drainage Area (acres) ; • Step 1. Determine the tailwater depth from channel characteristics below the pipe outlet for the design capacity of the pipe. If the tailwater depth is less than half the outlet pipe diameter,it is classified minimum tailwater condition_ If it is greater than half the pipe diameter it is classified maximum condition_ Pipes that outlet onto wide flat areas with no defined channel are assumed to have a minimum tailwater condition unless reliable flood stage elevations ' show otherwise. Outlet pipe diameter, Do (in.) 18 Tailwater depth (in.) 12 Minimum/Maximum tailwater? Max TW-(Fig. 8.06b)' Discharge (cfs) 6, Velocity (ft./s) _ 4.6 Step 2. Based on the tailwater conditions determined in step 1, enter Figure 8.06a or Figure 8.06b,and determine d50 riprap size and minimum apron length (La). The d .size is the median stone size in a well-graded riprap apron_ Step 3. Determine apron width at the pipe outlet,the apron shape, and the apron width at the outlet end from the same figure used in Step 2. Minimum TW Maximum TW w :3,. 'F Figure.8.06a a `, y: .figure 8 06b a Riprap d50, (ft.) 0.1 t i Minimum apron length, La (it) 9 Apron width at pipe outlet (ft.) 4.5 4:5 Apron shape Apron width at outlet end (ft.) 1.5 - 5.1 Step 4. Determine the maximum stone diameter: drn K = 1.5xdso Minimum TW Maximum TW Max Stone Diameter, dmax (ft) 0 -. 0.15 Step 5. Determine the apron thickness: Apron thickness = 1 5 x dmax Minimum TW Maximum TW Apron Thickness(ft.) 0 0.225- Step 6. Fit the riprap apron to the site by making it level for the minimum length, L . from Figure 8_06a or Figure 8_06b_ Extend the apron farther downstream and along channel banks until stability, is assured. Keep the apron as straight as possible and align it with the flow of the receiving stream. Make any necessary alignment bends near the pipe outlet so that the entrance into the receiving stream is straight. Some locations may require lining of the entire channel cross section to assure stability. It may be necessary to increase the size of riprap where protection of the channel side slopes is necessary (Appendix S.05)_ Where overfalls exist at pipe outlets or flows are excessive, a plunge pool should be considered, see page 8.06.8. • t DESIGN OF RIPRAP OUTLET PROTECTION User Input Data • 'Calculated Value -= Designed By: ;JAN, PE Date: 3/28/2017, Checked By: Date: Company: :Larry King,&Assoc, Project Name: The Crossings at,Cumberland Project No.: Site Location (City/Town) Fayetteville, NC - Culvert Id. FES-3 Total Drainage Area (acres) Step 1. Determine the tailwater depth from channel characteristics below the pipe outlet for the design capacity of the pipe. If the tailwater depth is less than half the outlet pipe diameter,it is classified minimum tailli.Tater condition. • If it is greater than half the pipe diameter, it is classified maximum condition_ Pipes that outlet onto wide flat areas with no defined channel are assumed to have a minimum tailwater condition unless reliable flood stage elevations show otherwise. Outlet pipe diameter, Do (in.) 18 - Tailwater depth (in.) 12 Minimum/Maximum tailwater? Max TW.(Fig.'8.06b) - Discharge (cfs) 6 Velocity (ft./s) 4,6, Step 2. Based on the tailwater conditions determined in step 1, enter Figure 8.06a or Figure 8.06b,and determine d50 riprap size and minimum apron length (La). The dm size is the median stone size in a well-graded riprap apron. Step 3. Determine apron width at the pipe outlet, the apron shape, and the apron width at the outlet end from the same figure used in Step 2. Minimum TW Maximum TW .'-��-�=''Figure�8.06az`��k`�;- �,< •Figurer_8�08b�r��- Riprap d50, (ft.) 0.1 Minimum apron length, La (ft.) , 9 Apron width at pipe outlet (ft.) 4.5 4.5 Apron shape Apron width at outlet end (ft.) 1.5 5.1- Step 4. Determine the maximum stone diameter: dam.= .5 x 60 Minimum TW Maximum TW Max Stone Diameter, dmax (ft.) 0 0.15 Step 5. Determine the apron thickness: Apron thickness = -1_5 x dry, Minimum TW Maximum TW Apron Thickness(ft.) 0 0.225 Step 6. Fit the riprap apron to the site by making it level for the minimum length, L�, from Figure 8_06a or Figure S.O6b. Extend the apron farther downstream and along channel banks until stability is assured. Keep the apron as straight as possible and align it with the flow of the receiving stream_ Make any necessary alignment bends near the pipe outlet so that the entrance into the receiving stream is straight_ Some locations may require lining of the entire channel cross section to assure stability It may be necessary to increase the size of riprap where protection of the channel side slopes is necessary (Appendix 8.05). Where overfalls exist at pipe outlets or flows are excessive, a plunge pool should be considered, see page 8.06.5. • DESIGN.OF RIPRAP:OUTLET PR TECTI I User Input Data , Calculated Value Designed By: JAN, PE Date: 3/28/2017 Checked By: Date: Company: Larry King &Assoc, Project Name: The`Crossings at Cumberland Project No.: Site Location (City/Town) Fayetteville, NC Culvert Id. Infil Basin #3 Total Drainage Area (acres) Step I. Determine the tailwater depth from channel characteristics below the pipe outlet for the design capacity of the pipe. If the tailwater depth is less than half the outlet pipe diameter,it is classified minimum tailwater condition. If it is greater than half the pipe diameter, it is classified maximum condition_ Pipes that outlet onto wide flat areas with no defined channel are assumed to have a minimum tailwater condition unless reliable flood stage elevations show otherwise. Outlet pipe diameter, Do (in.) 18 Tailwater depth (in.) 12 Minimum/Maximum tailwater? Max TW (Fig. 8.06b) Discharge (cfs) 6, Velocity (ft./s) 4:6' Step 2. Based on the tailwater conditions determined in step 1, enter Figure 8.06a or Figure 8.O6b,and determine cl5G riprap size and minimum apron length (La). The d,s size is the median stone size in a well-graded riprap apron_ Step 3. Determine apron width at the pipe outlet, the apron shape, and the apron width at,the outlet end from the sane figure used in Step 2. Minimum TW Maximum TW Figure 8:06a' ', %Ffgure-0:08bF<: ;` Riprap d50, (ft.) 0.1' 5 Minimum apron length, La (ft.) 9 Apron width at pipe outlet (ft.) 4.5 4.5 - Apron shape Apron width at outlet end (ft.) 1.5 5.1 Step 4. Determine the maximum stone diameter: dax = '1.5xdsa Minimum TW Maximum TW Max Stone Diameter, dmax (ft.) 0 0.15 Step 5. Determine the apron thickness: Apron thickness = t5 x d.. Minimum TW Maximum TW Apron Thickness(ft.) 0 - 0.225 Step 6. Fit the riprap apron to the site by making it level for the minimum length, La' from Figure 8.06a or Figure 8_06b_ Extend the apron farther downstream and along channel banks until stability is assured. Keep the apron as straight as possible and align it with the flow of the receiving stream_ Make any necessary alignment bends near the pipe outlet so that the entrance into the receiving strewm is straight_ Some locations may require lining of the entire channel cross section to assure stability It may be necessary to increase the size of riprap where protection of the channel side slopes is necessary (Appendix S.05). Where overfalls exist at pipe outlets or flows are excessive, a plunge pool should be considered, see page 8.06.8_ Appendix C F' \F'lb—II U SM11H—PACKLI ROCKFISH ROAD\CADD\CIVIL\P16-120\dwg\z—DRAINAGE AREA MAP dwg, 3/31/2017 2 40 44 PM, jnobles, 1 33 / 'n £ NN - ili 5 pp ggiiir t lif: g R g MAR -1NO � 1r' ,AN_rN rill ,❑=q , 75 Dog i91 A W , 31 I I 11®o®p.® 9(rx. a F \, \@� , �, ,,1�' \ I �\ I I ;11 , \\ I 1 J\ t e• \ n I \ / \ Z 1 I F I IX \ / I// / / 1 / Ia I I I: j3 I f II, c_%l If''2: ' i' e' 1 i 1:1111.—\ tr-,,,,. .„. _ ,441:11£".'' --rittl., „- 1 �+�2' i�x T Lr l e a 41 1 III`\ 4Yn,Td 1Y� d} 1�� 1 Yd I % 3" 1.1:14 714 Or F ill g 2 6 r `1' "TA i 21 1<21 1 vi II`,--rt 1 ; + F 714.114, °' ii _ 1 i 2 R~ 7 ,�•i i .. .� �� a SI T fr. t � yi'yi_�f yS�tr ° 6110,„mill"eF1r3I i? 4 I ,4411/4-41 rzi lTic I. i zit I1r a. !7 1di -M- V1thR1i ; - ry 1 t 1 Ipt7 _41/JIIII ( 4.-\ ' ire i "Mai 071), •r;,......=. 1411 0 Ill ; I ' I 42E i 416 :171-t /eye i,)Vi :g �F I I r • 1 �' 1 3 ; d E_ i z a C}C 1[0 s „r ®r.-.7a;=.77.17;,PA 'P E R I:Ip e o n 11`•ga m a 90 Box 53787 yV� D 5 P h�17 9 ti zA 3 'af gOit,s 13il hb,Om�on Road s,n1e 201 L `?G a F L-�H "' L`Y9 h y &',111; fwenevdle Na,m cmor o 28305 ['y7[',� yy P 19101 483 4302 F 1910)48".,0.52 z _-`a c y N !B - a��[. NC FrLKondA com-0BRI hh77 a g � + www 1 3/30/2017 CCJPB Map i'ftg f ' Cumberland County Planning Department 1 M (..' to* r�;' Fayetteville,North Carolina The Crossings at Rockfish Parcel Data Created by Public on Thursday,30 March 2017 k 'v,4 L^:_�„,"':;, -+( ✓`� ;rsi i ` - ,,,..• '- Illy--r_T -------11 i:13.1 ' - "i i 1 li ii I ..1 !inkit I CUD' r —"�I 02E \s ` ,,. 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Frontage Depth,Acres Acreage Value Value 9494-JOHNSON 6834 CAMDEN 96- BARBARA RD 02856 0539 $633702 $614709 $0 0 ft. 0 ft. 66.08 65.94 1873 M FAYETTEVILLE NC 28306 Table: Zoning Info [Count: 1, Base: 1] Case#Zone_Class Conditional Use Pin Owner Name Disclaimer RR 9494-96-1873-JOHNSON,BARBARA M Call(910)678-7603 to Verify Zoning Classification Table: Hyperlink to Assessor Data [Count: 1, Base: 1] Table: Register of Deeds Plat Image [Count: 1, Base: 1] Table: Register of Deeds Deed Image [Count: 1, Base: 1] Table: Virtual Maps Page [Count: 1, Base: 1] Centered On... 9494-96-1873- Table: 911 Address and Zip Code Lookup [Count: 1, Base: 1] 911 Address Assignment Date 6850 CAMDEN RD 06-11-1998 Table: 2030 Land We Plan [Count: 1, Base: 1] 2030 Land Use Urban Area Table: Area Plans Details [Count: 5, Base: 1] Detailed Plans Land Use Low Density Residential Open Space Office Institutional&Parks Medium Density Residential Heavy Commercial Table: Municipal Influence Area [Count: 1, Base: 1] Municipal or Farmland A rea Hope Mills Table: Within Urban Services Area or Farmland [Count: 1, Base: 1] Area Name urban area About This Map Disclaimer This map has been created for the purpose of showning Planning This map is a representation of the information currently held by information in Cumberland County.Any error should be reported to the Cumberland County.While every effort has been made to ensure the Cumberland County Joint Planning Dept.at accuracy of the product,Cumberland County accepts no responsibilityfor www.co.cumberland.nc.us/ping/staff.html. any errors or ommisions.Any feedback on ommisions or errors would be appreciated. t 3/30/2017 CCJPB Map "g: , `k` Cumberland CountyPlanningDepartment itl*c •t� . � ' k‘' Fayetteville,North Carolina mss,..s The Crossings at Cumberland Zoning Map Created by Public on Thursday,30 March 2017 ti *'-:----..--.1,-z-- ,y.,- »�_ —7 1'' i ---i i1 al\ ', \ ` v"" —7-- 1-.."- )1 1 1 tt�;�c S541 Q J_— _--�_ _ .� 'L.S. -y_" ti ids, i.,r7, li,ftl,i�`rfl pr_i_._ _____ I ,_____y______,.._____. il iLL 1LrT,S -iu T:°14`Y-�:✓:..•--.-, �! i'1 _ t .I 1-' — 1_tl-jrJT I,'l'ill i!)a"IJ i;�la-lv",`� :f:1-,„,-1,,,,,....,....a,.�1 ---- — ;! i'-ail_ 1CIIii J�,L71''. e.,Jd.I2 1 .-ti= ., - ,i -qI d F ,. 1,; ,;izla �,,rr�lrl4�>�J ii�i t,'141J la_J�_Js IJ ry f `�,- 1 t�-,i� , -��-r.l �'4 �'' ,ll�Ju-lh =is-la1 i��e lirle-7a=luiu- ��- ���� ((( -�; II '" E�,,i`'i,i India,'1",ra irrla_ilLificiq Y,n g' ' I lr1"7"0121i 1iltirinrPr'' p,.— ' I x1:y",., 11 ''I,` — _"( ,Dr _ifirli-1'cto J=licitiv i. t - -1' ';i I y«°i,']n„"l,l >)• ��—_� _ �=j�y '1111-,,-i4,4,-62,, i1 1a IG-IIi liJu,r-III i I� ffiEti �I. :-`; _ -�. ��i��} ++ ,_L+___+' ._ i' _._ ���R 11-1 0, ,ICj�' ,,-�+•2,, ii-b G_l� 'Ilir;_wS!' , _ ' hlige�l! ,I -- �riC� � 1✓Il�ltl�E _ ��4!�, ill lIl ,„4 1'-' Oreo asiv�nt'i �I w 1® l `'' :0 ��; e'r�PTiil lit ;a lillu-Ir�-.J7i,-_1 - - li _ ?4�ir4��till, bt. ., Il� +CIri; la 11 . s,i' 64111 a'L. ,- rtTr ----,.. 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Box 9321 Fayetteville,NC 28311 Phone/Fax(910) 822-4540 Email mike @ southeasternsod.com December 242016 Mrs. Lori Epler Larry King&Associates; RLS,PA 1333 Morganton Road, Suite 201 Fayetteville,NC 28305 Re: Hydraulic conductivity(permeability) analysis&seasonal water table determination(SHWT)for proposed stormyvater retention area, Smith Packett Project, Rockfish Road, Cumberland County,North Carolina Dear Mrs. Epler; An evaluation of:soil properties.and hydraulic conductivity(Ksat)has been conducted at your request on the aforementioned property. The purpose of the investigation was to determine soil water table depths(SHWT)based on soil profiles. In addition,Ksat was to be provided ata depth 2.0 feet above the-SHWT elevation for use vvith.stotmwater retention basin design. Saturated hydraulic conductivity of the unsaturated zone was measured in a similar method as described in the Soil Science Society of America Journal,Vol. 53,no 5, Sept. - Oct. 1989, "A-Constant Permeameter for Measuring Saturated.Hydraulic Conductivity of the Vadose Zone' and Comparison of the Glover Solution with the Simultaneous Equations Approach for Measuring Hydraulic Conductivity." This consists of advancing a small diameter bore hole to a predetermined depth(typically 2 feet above SHWT). At this depth,a constant head(pressure)was established and maintained. Flow measurements were made at timed intervals after flow stabilized. Soils at the proposed basin-site are most similar to the,Autryville soil series (see attached boring logs). Three borings were advanced to at least 8.0 feet below the soil surface. Seasonal High Water Table(SHWT) as determined by evidence of colors of chroma 2 or less(and/or concentrations of high redox mottles)was encountered at depths ranging from 49 to 69 inches below the ground surface(see chart attached). SOIUSITE EVALUATION •SOIL PHYSICAL ANALYSIS'•LAND USE/SUBDIV1SION PLANNING•WETLANDS GROUNDWATER DRAINAGE/MOUNDING•SURFACE/SUBSURFACE WASTE TREATMENT SYSTEMS, EVALUATION&DESIGN { 5 Three compact constant head permeameter(CCHP)tests were conducted at depths of 2.00 feet above the SHWT level. The measured_IKsat rates ranged between 1.29 and 29.27 em/hr(equivalent to 0.51 to 11.52 inches/hour). The attached map 'shows locations of the sample points as well as.Ksat locations. It should be noted that the-reported SHWT does not necessarily reflect the.elevation of static groundwater(due to variations in groundwater recharge rates,animal rainfall, drought conditions, etc.). The-data p•resented in this report are limited by a number of considerations. The primary consideration is'that soil formations can be.highly variable. The soils found on.this,site can be subject to inclusions of other soil types,perched water, artesian conditions and/or layers ofundulating low permeability clay seams. These and other soil conditions can have an effect on the steady state of groundwater flow. To the extent possible,lwe have identified the soil types that will impact the flow of groundwater,and have provided a professional opinion as,to the depth of SHWT. I trust this is the information you require at this time. Sincerely, SOIL Mike Eaker ` ' t~l_D NC'Licensed Soil Scientist#1030 f ' ° 04,0 d Mem ! � 1i• 4... ayy `� r 101 • .eft Y, � 4' t J } t L Southeastern o l fEnviron .o.1 issociAes, inc. PLO.Box 9321 Fayetteville, NC 28311 Phone/Fax(910)822-4540 Email mike@Southeasternsoil.com Measured Ksat Rates, Smith Packett, Rockfish.Road, Cumberland County,NC Ksat Ksat Location Depth (in) cmihr in/hr 1 25 1.29 0.51 2 45 9.90 3.89 3 36 29.27 11.52 SOIUSITE EVALUATION I SOIL PHYSICAL ANALYSIS LAND USE/SUBDIVISION PLANNING•WETLANDS GROUNDWATER DRAINAGE/MOUNDING•SURFACE/SUBSURFACE WASTE TREATMENT SYSTEMS,EVALUATION&DESIGN Southeastern Soil & Environmental Associates, Inc. 'RO,Box 9321 Fayetteville,NC 28311 Phone/Fax(910)822-4540 Email mike@southeastemsoiLcom SIIWT depths, Smith Packett,Rockfish,Road, Cumberland County, NC BORING SHWT;DEPTH(inches) Observed Water(inches) 1 49 48 2 69 75, 3 62 69 SOIUSITE EVALUATION c SOIL"PHYSICAL"ANALYSIS'LAND USE/SUBDIVISION PLANNING c WETLANDS GROUNDWATER.ORAINAGE/MOUNDING 6 SURFACE/SUBSURFACE'WASTE TREATMENT SYSTEMS,EVALUATION&DESIGN t • Southeastern Soil & EnvironSental A'ssoci tes9 enc® PO. Box 9321 Fayetteyille, NC 28311 Phone/Fax(910)822-4540 Email mike@squtheasternsoll.com, Typical Soil Boring Log,Smith Packett Project,Rockfish Road,Cumberland County,NC This map unit consists of well drained soils that formed in loamy sediments on uplands. Slopes range from 0 to 1 percent. A- 0 to 9 inches; dark grayish brown(10YR 4/2)loamy sand;weak fine granular structure;very friable;common-fine and medium roots;abrupt smooth boundary. E- 9 to 22 inches; light yellowish brown,(10YR.6/4) sand;weak medium granular structure; very friable;few fine roots; clear•smooth boundary. Btl -22 to 39 inches;brownish yellow(10YR 616) sandy loam;weak fine subangular blocky structure;,friable; gradual wavy boundary. Bt2 -39 to 65-inches; brownish yellow(10YR 6/6) sandy loam;many medium prominent reddish yellow(5YR 6/8)mottles;weak fine granular structure;very friable; gradual wavy boundary. BC -65 to 69 inches; brownish yellow(10YR 6/6) sandy loam;many medium prominent reddish yellow(5YR 6/8)and few fine prominent gray(10YR 6/1)mottles; weak fine granular structure;very friable; gradual wavy boundary. C- 69 to'96 inches;mixed mottled reddish yellow (5YR 6/8)and gray (10YR 6/1) loamy sand;friable;massive structure. SHWT @ 49-inches (10YR 6/1)in boring 1 SHWT @ 69 inches(10YR 6/1)in boring,2 SIIWT @ 62 inches(10YR 6/1) in boring 3 SOIUSITE EVALUATION •SOIL PHYSICAL ANALYSIS•LAND USE/SUBDIVISION PLANNING•WETLANDS GROUNDWAI-ER DRAINAGE/MOUNDING•SURFACE/SUBSURFACE WASTE TREATMENT SYSTEMS,EVALUATION&DESIGN i e. _ theastt xia -!,...`4-11-- ., }ir - < e } t `t 0.; s ; "`&'S i a.,-.--5, .+S I is .P.O. B'ox 9321 Fayetteville,NC ,1 _ _ _ --" Phone/Fax(910)822-4540 L_ Email mike @ southeasternsoiLcom — r I � N4480n i. I rt,e1------ / i / I I s-7 721 i 1 I _J 1 1e- 1 X N44700 _ X )C - �'' L. I 1 \ , \ , 1 1 1 \ ...,..-- , t. - _ .„_] - 1 Soil Boring/Ksat Location, Smtih Packett Project Rockfish Road, Hope Mills, NC US State Plane-1983 Scale 1:4,000 R121909A.SSF North Carolina 3200 N NAD 1983(Conus) 0 500.0 12/21/2016 I E W___ GPS PathfinderOffice II Feet 60-Trimble. 1 SOIUSITE EVALUATION •SOIL PHYSICAL ANALYSIS 0 LAND USE/SUBDIVISION PLANNING•WETLANDS GROUNDWATER DRAINAGE/MOUNDING•SURFACE/SUBSURFACE WASTE TREATMENT SYSTEMS,EVALUATION&DESIGN � 5 Southeastern ..: . 118LE vironm ::..ntal :: . ;• iates9 Inc P.O. BoX 9321 Fayetteville,NC 28311 Phone/Fax(910)822-4540 Email mike@southeasternsoil.com February 28,2017 Mr. Jeffrey Nobles,PE Larry King&Associates,RLS,PA 1333 Morganton Road, Suite 201 Fayetteville,NC 28305 Re: Additional hydraulic conductivity(permeability) analysis & seasonal water table determination(SHWT)for potential stormwater retention areas,'Smith Packett Project, Rockfish Road, Cumberland County,North Carolina Dear Mr.Nobles, An evaluation of soil properties and hydraulic conductivity(Ksat)has been conductedat your request on the aforementioned property. The purpose of the investigation was to determine soil water table depths(SHWT)based on soil profiles. In addition, I(sat was to be provided at a depth of at least,2.0 feet above the SEIWT elevation for use with stormwater retention basin design. Saturated hydraulic conductivity of the unsaturated zone,was measured in a similar method as described in the Soil Science Society of America Journal,Vol. 53,no 5, Sept. - Oct..1989,"A Constant Per neameter for Measuring Saturated Hydraulic Conductivity of the Vadose Zone"and Comparison of the Glover Solution with the Simultaneous Equations Approach for Measuring Hydraulic Conductivity." This consists of advancing a small diameter bore hole to a predetermined depth(typically 2 feetabove SHWT). At this depth,a constant head(pressure)was established and maintained. Flow measurements were made at timed intervals after flow stabilized. Soils at the proposed basin site are most similar to the Autryville soil series (see attached boring logs). Three additional borings were advanced to 8.0 feet below the soil surface. Seasonal High Water Table,(SHWT) as determined by evidence of colors of chroma 2 or less(and/or concentrations of high redox mottles)was encountered at depths ranging from 51 to 82 inches below the ground surface (see chart attached). SOIL/SITE EVALUATION •SOIL PHYSICAL ANALYSIS•LAND USE/SUBDIVISION PLANNING•WETLANDS GROUNDWATER DRAINAGE/MOUNDING•SURFACE/SUBSURFACE WASTE TREATMENT SYSTEMS,EVALUATION&DESIGN Three compact,constant head permeameter(CCHP)'tests were conducted at depths of at least 2.00.feet above the SHWT level The:measured Ksat rates ranged between 7.983 and 27.489 cm/hr(equivalent to 3.143 to 10.822 inches/hour). The attached map shows locations of the sample points as well as.Ksatlocations. It should be noted-that the reported SHWT does-not i eceSsarily reflectthe elevation of static groundwater(due to variations in groundwater recharge rates,-annual rainfall, drought conditions, etc.). The,data presented in this report are limited by a number of considerations. The primary consideration:is that soil formations can be highly variable. The soils found on this site can be subject to inclusions of other soil,types,perched water,artesian conditions and/or layers of undulating low permeability clay seams. These and other soil conditions can have an effect on the steady state-of groundwater flow. To the extent possible,we have identified the soil types that will impactthe flow of groundwater,and have provided a professional opinion as to the depth of SHWT. I trust this is the information you require at this time. Sincerely, ‘11426-(--- $®dL Mike Faker -E ` tom,` NC Licensed Soil Scientist#1030 *... v . • RriffIVTiett. 1 e ifteW a I 1 � Southeastern Soil & Environmental Ass ciates, Inc. P.O.Box 9321 Fayetteville, NC 28311 Phone/Fax(910)822-4540 Email milce@southeastemsoll.cpm Measured-Ksat Rates, Smith Packett,Rockfish Road, Cumberland County,NC Ksat Ksat Location Depth (in) cm/hr in/hr 4 58 27.489 10.822 5 44 7.983 1143 6 27 25.946' 10.215 SOIL/SITE EVALUATION •SOIL PHYSICAL ANALYSIS•LAND USE/SUBDIVISION PLANNING•WETLANDS GROUNDWATER DRAINAGE/MOUNDING•SURFACE/SUBSURFACE WASTE TREATMENT-SYSTEMS;EVALUATION&DESIGN Southeastern Soil & EnvironmentalAssociates1 Inc. P.O.Box 9321 - Fayetteville, NG 28311 Phone/Fax(91Q),822-4540 Email mike @southeasternsoil,com SHWT depths, Smith Packett Project,Rockfish 1oad,,Cuinberiand County,NC BORING SHWT DEPTH(inches) SHWT DEPTH("ms1Z 4 82 175.52 -5 68 176,59 -6 51 176.72 SOIL/SITE EVALUATION a SOIL Pt1Y5ICALANALYSIS a LAND USE/SUBDIVISION PLANNING•WETLANDS GROUNDWATER DRAINAGE/MOUNDING•SURFACE/SUBSURFACE WASTE TREATMENT SYSTEMS,EVALUATION&DESIGN Southeastern Soil Environmental rr cit _sInce P.O.Box 9321 Fayetteville, NC 28311 Phone/Fax(91(4822-4540 Email mike@southeasternsoil.com Typica1Soil BoringLog,Smith Packett Project,Rockfish Road,Cumberland County,NC This map unit consists of well drained soils that formed in loamy sediments on uplands. Slopes range,from 0 to 1 percent. A-0 to 8 inches; dark grayish brown(10YR 4/2) loamy sand;weak fine granular structure;very friable; common fine,and medium roots; abrupt,smooth boundary. E- 8.to 20 inches;light yellowish brown(10YR 6/4) sand;weak medium granular structure;very.friable; few,fine roots; clear smooth boundary. Bt—20 to 35 inches;brownish yellow(10YR 6/6,) sandy loam;weak fine,subangular blocky structure;friable; gradual wavy boundary. E' -35 to 68 inches; brownish yellow(10YR 6/8) sand; single grained; loose; common medium pockets of'clean sand grains; gradual wavy boundary. BC 68 to 78 inches;brownish yellow(10YR.6/8)loamy sand; common medium distinct red(2.5YR 4/8)and light gray(10YR 7/1)mottles;massive structure; very friable; gradual wavy boundary. C -78 96 inches;,light,gray(-10'YR 7/1) coarse sand;many medium prominent brownish yellow(10YR 6/8)mottles;very friable;massive structure. STTWT @ 82•inches in boring 4(10YR 3/2) SHWT @ 68 inches in boring 5 (10YR 7/1) SHWT @ 51 inches in boring 6(10YR 7/1) SOIUSITE EVALUATION o SOIL PHYSICAL ANALYSIS°LAND USE/SUBDIVISION PLANNING-WETLANDS GROUNDWATER DRAINAGE/MOUNDING•SURFACE/SUBSURFACE WASTE TREATMENT SYSTEMS,EVALUATION&DESIGN 1•\I•I11•IYU,,1111-'AUkLI'PM Mr 111I ICUAU\C'Nl UVI/VI 6\I'I6-ILO\dwq\OOJ-C,ICAUI;.,UICAIN.dwO,?/21/_3017 6.48 3! PA.1661.10y, I.3$6326 qif, ii.Fn' A\ , r .j_.I I I \ \-i\'\\ .1 ak i :i'. 1. ..-a ) '-,/ , / 1 - Vrel.. ,,./ ` 7 a / 9 . . Ly _�._,S" y a, o . o- i f- ig 111li-:1 iPTIP'MPO' .'f ...4..2{1':IT IL\\\‘` c.---- le ;;1;1 .,\... ' 14 la iii I 6.h T. 1' Vy:__.. ,1� QygY' m ,i I W' /I it' ii 6 V.' 1, • ________________ '• '6.0-'4 \ /,i' fi— V£ — A , 1 ffi _2 / . ... :`,• 6 e 'er ' . .1 i.--:03 -,•,', i Fa ! —' 2. 1 .i.:` F. i tl ;1 fA -Cle',3-:mih 2E mai i , e. - PE ti 111E �1y ° § ' .T 0 ®ten a�6 i asmclolcls LIS..P.a,1t1y1I�� " ?..z.,3-,,, /: [k]a 1:-,E.'43 ,9,M - 1 .6 :f ¢¢ggxx 1XCNa 'Raad ftla:Ol CF77 '''ll1S kr.n�.wa:ncwrro.x7os W 4 2 c 2 9 Z 9 0 >•''E T v, in, $ 3 r Mop.m�f.1v1aId1•� g I ry x fi, ' g° H l rlC® A. 9 Appendix E 2856 0539 - .• tnOY98 ��++ 5U 1 nE539 t` Exet,e Tax 0 0 Recording Time.Book tad Page Tax Lot No. . _ Parcel Identifier No. Verified by County on the. day of - . ,19. by .. ... . . . . - - Mail after recording to John Blackwell, Jr. „ , „ P,O. Box 469, Fayetteville, Nc,28302 , This Instrument was prepared by John Blackwell, Jr, • . Brief description for the Index Tracts, Rockfish Twp NORTH CAROLINA NON-WARRANTY DEED THIS DEED made the 30th day of October 19 81 ,by and between GRANTOR GRANTEE BARBARA M. JOHNSON, Executrix BARBARA M. JOHNSON of the Estate of John Gilbert Rt Fayettev2 ille, NC 28306 Johnson L - Tatar to appeapdate Meek for each party:name,address,ad.If appnpoiale,dander of entity,eq.corporation or partnenkip. The designation Grantor and Grantee as used herein shall include acid parties,their heirs,,uccessors,and assigns,and shall include singular,plural,masculine,feminine or neuter a,required by context. WITNESSETH,that the Grantor, for a valuable consideration paid by the Grantee, the receipt of which is hereby acknowledged,has and by theme presents does grant,bargain,,ell and convey unto the Grantee in fee simple,all that ROCkfi sh Township certain lot or parcel of land situated In ,the City of- Cumber;and County,North Carolina and more particularly described ns foliose: FIRST TRACT: BEGINNING at a stake in the old Baker line, it being the Northeast corner of the tract of which this is a part, and runs thence with the old line South 1 degree 30 minutes West B chains and 22 links to a stake; thence North 87 West, 36 chains and 50 links to a stake in the old line; thence North 1 degree 30 minutes East 8 chains 22 links to a stake an old corner; thence with another old line South 87 degrees East 36 chains and 50 links to the beginning containing 30 acres, more or less. SECOND TRACT; _BEGINNING at a stake on the south side of the Wire Road, and running thence North 3 degrees West 42 chains to a corner, black jack pointers; thence West 20 chains to a corner, in the head of a branch; „ . thence South 3 degrees East 3 chains to a corner; thence South 5 degrees East 18 chains 50 links to a corner; thence South 70 degrees East 16 chains 31 links to a corner; thence South 5 degrees East 23 chains 50 links to a corner; thence North 85 degrees East 26 chains to the beginning, containing 13511 acres, more or less. There is excepted from the Second Tract the 6 acres as excepted in Deed recorded in Book 2405, Page 706, Cumberland County Registry. n C Nur weave.r.m Ne 1 L 1111 • 1